Borehole conductivity simulator verification and transverse antenna balancing

ABSTRACT

A reactance is introduced into a flow path of axial currents in an induction logging tool. The reactance may be a capacitor or an inductor. A transmitter antenna is operated at a frequency defined by a cutoff frequency related to the reactance.

CROSS REFERENCE TO RELATED APPLICATIONS

The present application is a continuation-in-part of and claims priority from U.S. patent application Ser. No. 11/627,172 which is a continuation-in-part of and claimed priority from U.S. patent application Ser. No. 11/371,052 filed on the Mar. 8, 2006, claiming priority from U.S. patent application Ser. No. 10/841,397 filed on May 7, 2004, and U.S. patent application Ser. No. 11/340,785 filed on Jan. 26, 2006.

BACKGROUND OF THE DISCLOSURE

1. Field of the Disclosure

The present disclosure is related to the field of apparatus design in the field of oil exploration. In particular, the present disclosure describes a method for calibrating multicomponent logging devices used for detecting the presence of oil in boreholes penetrating a geological formation.

2. Description of the Related Art

Electromagnetic induction resistivity well logging instruments are well known in the art. Electromagnetic induction resistivity well logging instruments are used to determine the electrical conductivity, and its converse, resistivity, of earth formations penetrated by a borehole. Formation conductivity has been determined based on results of measuring the magnetic field of eddy currents that the instrument induces in the formation adjoining the borehole. The electrical conductivity is used for, among other reasons, inferring the fluid content of the earth formations. Typically, lower conductivity (higher resistivity) is associated with hydrocarbon-bearing earth formations. The physical principles of electromagnetic induction well logging are well described, for example, in, J. H. Moran and K. S. Kunz, Basic Theory of Induction Logging and Application to Study of Two-Antenna Sondes, Geophysics, vol. 27, No. 6, part 1, pp. 829-858, Society of Exploration Geophysicists, December 1962. Many improvements and modifications to electromagnetic induction resistivity instruments described in the Moran and Kunz reference, supra, have been devised, some of which are described, for example, in U.S. Pat. No. 4,837,517 to Barber, in U.S. Pat. No. 5,157,605 to Chandler et al., and in U.S. Pat. No. 5,600,246 to Fanini et al.

The conventional geophysical induction resistivity well logging tool is a probe suitable for lowering into the borehole and it comprises a sensor section containing a transmitter and receiver and other, primarily electrical, equipment for measuring data to infer the physical parameters that characterize the formation. The sensor section, or mandrel, comprises induction transmitters and receivers positioned along the instrument axis, arranged in the order according to particular instrument or tool specifications and oriented parallel with the borehole axis. The electrical equipment generates an electrical voltage to be further applied to a transmitter induction antenna, conditions signals coming from receiver induction antennas, processes the acquired information, stores or by means of telemetry sending the data to the earth surface through a wire line cable used to lower the tool into the borehole.

In general, when using a conventional induction logging tool with transmitters and receivers (induction antennas) oriented only along the borehole axis, the hydrocarbon-bearing zones are difficult to detect when they occur in multi-layered or laminated reservoirs. These reservoirs usually consist of thin alternating layers of shale and sand and, oftentimes, the layers are so thin that due to the insufficient resolution of the conventional logging tool they cannot be detected individually. In this case the average conductivity of the formation is evaluated.

Conventional induction well logging techniques employ antennas wound on an insulating mandrel. One or more transmitter antennas are energized by an alternating current. The oscillating magnetic field produced by this arrangement results in the induction of currents in the formations which are nearly proportional to the conductivity of the formations. These currents, in turn, contribute to the voltage induced in one or more receiver antennas. By selecting only the voltage component which is in phase with the transmitter current, a signal is obtained that is approximately proportional to the formation conductivity. In conventional induction logging apparatus, the basic transmitter antenna and receiver antenna has axes which are aligned with the longitudinal axis of the well logging device. (For simplicity of explanation, it will be assumed that the borehole axis is aligned with the axis of the logging device, and that these are both in the vertical direction. Also single antennas will subsequently be referred to without regard for focusing antennas or the like.) This arrangement tends to induce secondary current loops in the formations that are concentric with the vertically oriented transmitting and receiving antennas. The resultant conductivity measurements are indicative of the horizontal conductivity (or resistivity) of the surrounding formations. There are, however, various formations encountered in well logging which have a conductivity that is anisotropic. Anisotropy results from the manner in which formation beds were deposited by nature. For example, “uniaxial anisotropy” is characterized by a difference between the horizontal conductivity, in a plane parallel to the bedding plane, and the vertical conductivity, in a direction perpendicular to the bedding plane. When there is no bedding dip, horizontal resistivity can be considered to be in the plane perpendicular to the bore hole, and the vertical resistivity in the direction parallel to the bore hole. Conventional induction logging devices, which tend to be sensitive only to the horizontal conductivity of the formations, do not provide a measure of vertical conductivity or of anisotropy. Techniques have been developed to determine formation anisotropy. See, e.g. U.S. Pat. No. 4,302,722 to Gianzero et al. Transverse anisotropy often occurs such that variations in resistivity occur in the azimuthal direction.

Thus, in a vertical borehole, a conventional induction logging tool with transmitters and receivers (induction antennas) oriented only along the borehole axis responds to the average horizontal conductivity that combines the conductivity of both sand and shale. These average readings are usually dominated by the relatively higher conductivity of the shale layers and exhibit reduced sensitivity to the lower conductivity sand layers where hydrocarbon reserves are produced. To address this problem, loggers have turned to using transverse induction logging tools having magnetic transmitters and receivers (induction antennas) oriented transversely with respect to the tool longitudinal axis. Such instruments for transverse induction well logging has been described in PCT Patent publication WO 98/00733 of Beard et al. and U.S. Pat. No. 5,452,761 to Beard et al.; U.S. Pat. No. 5,999,883 to Gupta et al.; and U.S. Pat. No. 5,781,436 to Forgang et al.

In transverse induction logging tools, the response of transversal antenna arrays is also determined by an average conductivity; however, the relatively lower conductivity of hydrocarbon-bearing sand layers dominates in this estimation. In general, the volume of shale/sand in the formation can be determined from gamma-ray or nuclear well logging measurements. Then a combination of the conventional induction logging tool with transmitters and receivers oriented along the well axis and the transversal induction logging tool can be used for determining the conductivity of individual shale and sand layers.

One, if not the main, difficulties in interpreting the data acquired by a transversal induction logging tool is associated with vulnerability of its response to borehole conditions. Among these conditions is the presence of a conductive well fluid as well as wellbore fluid invasion effects.

In induction logging instruments, the acquired data quality depends on the formation electromagnetic parameter distribution (conductivity or resistivity) in which the tool induction receivers operate. Thus, in the ideal case, the logging tool measures magnetic signals induced by eddy currents flowing in the formation. Variations in the magnitude and phase of the eddy currents occurring in response to variations in the formation conductivity are reflected as respective variations in the output voltage of receivers. In the conventional induction instruments these receiver induction antenna voltages are conditioned and then processed using analog phase sensitive detectors or digitized by digital to analog converters and then processed with signal processing algorithms. The processing allows for determining both receiver voltage amplitude and phase with respect to the induction transmitter current or magnetic field waveform. It has been found convenient for further uphole geophysical interpretation to deliver the processed receiver signal as a vector combination of two voltage components: one being in-phase with transmitter waveform and another out-of-phase, quadrature component. Theoretically, the in-phase antenna voltage component amplitude is the more sensitive and noise-free indicator of the formation conductivity.

There are a few hardware margins and software limitations that impact a conventional transversal induction logging tool performance and result in errors appearing in the acquired data.

The general hardware problem is typically associated with an unavoidable electrical field that is irradiated by the tool induction transmitter simultaneously with the desirable magnetic field, and it happens in agreement with Maxwell's equations for the time varying field. The transmitter electrical field interacts with remaining modules of the induction logging tool and with the formation; however, this interaction does not produce any useful information. Indeed, due to the always-existing possibility for this field to be coupled directly into the receiver part of the sensor section through parasitic displacement currents, it introduces the noise. When this coupling occurs, the electrical field develops undesirable electrical potentials at the input of the receiver signal conditioning, primarily across the induction antenna receiver, and this voltage becomes an additive noise component to the signal of interest introducing a systematic error to the measurements.

The problem could become even more severe if the induction logging tool operates in wells containing water-based fluids. The water-based mud has a significantly higher electrical permittivity compared to the air or to the oil-based fluid. In the same time, the electrical impedance to the above mentioned displacement currents can be always considered as capacitive coupling between the source—the induction transmitter and the point of coupling. This circumstance apparently would result in a fact that capacitive coupling and associated systematic errors are environment dependant because capacitive impedance will be converse to the well mud permittivity.

The conventional method in reducing this capacitive coupling in the induction logging instrument lays in using special electrical (Faraday) shields wrapped around both transmitter and receiver induction antennas. These shields are electrically attached to the transmitter analog ground common point to fix their own electrical potential and to provide returns of the displacement currents back to their source—transmitter instead of coupling to any other place in the tool. However, geometry and layout effectiveness of Faraday shields becomes marginal and contradictory in the high frequency applications where conventional transverse induction tools can operate. These limitations occur due to the attenuation these shields introduce to the magnetic field known in the art as a shield “skin effect”. The shield design limitations are unavoidable and, therefore, the possibility for the coupling through displacement currents remains.

Another source of hardware errors introduced into the acquired log data is associated electrical potential difference between different tool conductive parts and, in particular, between transmitter and receiver pressure housings if these modules are spaced apart or galvanically separated. These housings cover respective electronic modules and protect them from exposure to the harsh well environment including high pressure and drilling fluids. Typically, the pressure housing has a solid electrical connection to the common point of the electronic module it covers, however, design options with “galvanically” floating housings also exist. If for some reasons, mainly imperfections in conventional induction tools, the common points of different electronic modules have an electrical potential difference between them, this difference will appear on the pressure housings. It may occur even in a design with “galvanically” floating housings if the instrument operates at the high frequencies and, in particular, through the capacitive coupling that these metal parts might have to the electronic modules encapsulated in a conductive metallic package.

Having different electrical potentials on separate pressure housings will force the electrical current to flow between them. This current would have a conductive nature and high magnitude if the induction tool is immersed in a conductive well fluid and it will be a displacement current of typically much less magnitude for tool operations in a less conductive or oil-based mud. In both cases this current is time-varying; therefore it produces an associated time varying magnetic field that is environmentally dependent and measured by the induction receiver. For those who are skilled in the art it should be understood that the undesirable influence of those currents on the log data would be significantly higher in the conventional transverse induction tool compared to the instruments having induction antennas coaxial with the tool longitudinal axis only. In particular, this is due to the commonly accepted overall design geometry of induction logging tools where transmitter and receiver sections are axially separated by the mandrel. It can be noticed that employing the induction tool in the logging string where it has mechanical and electrical connections (including telemetry) with instruments positioned both above and below could also result in the appearance of the above-mentioned currents.

Another source of the housings' potential offsets is the induction tool transmitter itself. The remaining electrical field that this transmitter irradiates simultaneously with a magnetic field could be different on the surface of separate pressure housings. Severity of this error also depends on Faraday shields' imperfections as described earlier.

There is an additional problem that the potential difference creates in conventional tool layouts having transmitter and receiver electronic modules spaced apart and using interconnection wires running throughout the sensor (mandrel) section. These wires should be electrically and magnetically shielded from induction receiver antennas in the sensor section. The entire bundle of wires is placed inside of a highly conductive metal shield that is electrically connected to the common points of separated transmitter and receiver electronic modules. This shield's thickness is selected to enable sufficient suppression of mutual crosstalk between wires and sensor section antennas within the entire operational frequency bandwidth and, primarily, at its lower end. In some cases, this shield is a hollow copper pipe, often called as a feed-though pipe, with a relatively thick wall.

However, besides protecting the sensor section transmitter and receiver antennas and interconnecting wires from mutual crosstalk, this shield simultaneously creates a galvanic path for the currents that could be driven by pressure housings and/or electronic potential difference, or induced by the induction transmitter (as discussed in U.S. Pat. No. 6,586,939 to Fanini et al, having the same assignee as the present application and the contents of which are incorporated herein by reference). This path apparently exists along the shield's external surface and for a given frequency its depth and impedance has been controlled by the shield geometry, material conductivity and magnetic permeability. The time varying currents also generate a respective magnetic field that crosses induction receiver antennas and induces error voltages. Unfortunately, these error voltages are also environmentally dependent and their changes cannot be sufficiently calibrated out during tool manufacturing. The overall analysis of the potential difference influence demonstrates that in the conductive well fluid, galvanic currents flowing through the fluid along external surface of the induction tool would dominate. The superposition and magnitude of these galvanic currents strongly depend up on the ambient temperature that pushes the conventional induction tool performance to further deterioration.

Another source of systematic errors introduced in the log data is directly determined by uncertainties in mechanical dimensions of multi-component transmitter and receiver antennas in the sensor section related both to their overall dimensions and positions with respect to each other. Thus, to keep required signal phase relationships, conventional tool designs have primarily relied on the mechanical stability and electrical properties of advanced ceramics and plastic materials to build the mandrel. However, even slight physical assembly deviations in the antenna wires position and non-uniform antenna form material temperature dependencies might destroy a factory pre-set compensation of the transmitter primary magnetic field coupled in the receiver antenna (bucking) during well logging, and create non-recoverable errors due to mechanical displacement or imperfections.

U.S. Pat. No. 6,734,675 and U.S. Pat. No. 6,586,939 to Fanini et al., both having the same assignee as the present application and the contents of which are incorporated herein by reference, address some of the issues present in the calibration and use of multicomponent induction logging tools. Fanini '939 discloses a transverse induction logging tool having a transmitter and receiver for downhole sampling of formation properties, the tool having a symmetrical shielded split-antenna transmitter antenna and a bucking antenna interposed between the split transmitter antennas to reduce coupling of the transmitter time varying magnetic field into the receiver. The tool provides symmetrical shielding of the antennas and grounding at either the transmitter or receiver end only to reduce coupling of induced currents into the received signal. The tool provides an insulator between receiver electronics and the conductive receiver housing having contact with conductive wellbore fluid, to reduce parasitic current flowing in a loop formed by the upper housing, feed through pipe, lower housing and wellbore fluid adjacent the probe housing or mandrel. An internal verification loop is provided to track changes in transmitter current in the real and quadrature component of the received data signal.

Fanini '675 discloses a transverse induction logging tool having a transmitter and receiver for downhole sampling of formation properties, the tool having a symmetrical shielded split-antenna transmitter antenna and a bucking antenna interposed between the split transmitter antennas to reduce coupling of the transmitter time varying magnetic field into the receiver. The tool provides symmetrical shielding of the antennas and grounding at either the transmitter or receiver end only to reduce coupling of induced currents into the received signal. The tool provides an insulator between receiver electronics and the conductive receiver housing having contact with conductive wellbore fluid, to reduce parasitic current flowing in a loop formed by the upper housing, feed through pipe, lower housing and wellbore fluid adjacent the probe housing or mandrel. An internal verification loop is provided to track changes in transmitter current in the real and quadrature component of the received data signal.

SUMMARY OF THE DISCLOSURE

One embodiment of the disclosure is a method of preparing a multicomponent induction tool having a plurality of transmitter antennas and a plurality of receiver antennas. The method includes positioning the logging tool in a calibration area substantially free from components capable of interfering with magnetic and electric fields produced by the tool. A first conductive housing of the tool is coupled with a second conductive housing of the tool through a borehole conductivity simulator having an impedance similar to that of a borehole environment. A first antenna of the plurality of transmitter antennas is activated and the signal in a first antenna of the plurality of receiver antennas is measured. A reactance is introduced into an axial flow path for the currents and the transmitter is operated at a frequency related to a cutoff frequency defined by the introduced reactance.

Another embodiment of the disclosure is an apparatus for evaluating performance of the multicomponent induction logging tool having a plurality of transmitter antennas and a plurality of receiver antennas. The tool is positioned in a calibration area substantially free from components capable of interfering with magnetic and electric fields produced by the tool. The apparatus includes a borehole conductivity simulator having an impedance similar to that of a borehole environment, the borehole conductivity simulator coupling a first housing of the tool with a second housing of the tool. The apparatus includes a processor configured to activate a first antenna of the plurality of transmitter antennas. The apparatus further includes a first antenna of the plurality of receiver antennas configured to provide a signal responsive to the activation of the first transmitter antenna. The apparatus includes a reactance introduced in a flow of axial current to reduce the effect of the magnetic field produced by the axial current. The transmitter is operated at a frequency related to a cutoff frequency defined by the introduced reactance.

BRIEF DESCRIPTION OF THE DRAWINGS

The present disclosure is best understood with reference to the accompanying figures in which like numerals refer to like elements and in which:

FIG. 1 (prior art) shows schematically a wellbore extending into a laminated earth formation, into which wellbore an induction logging tool as used according to the disclosure has been lowered;

FIG. 2A (prior art) illustrates a conventional resistivity measurement in the vertical direction;

FIG. 2B (prior art) illustrates a resistivity measurement in the horizontal direction;

FIG. 3 is an overall flow chart of the procedures of the present disclosure;

FIG. 4 illustrates a borehole conductivity simulator (BCS) used in the present disclosure;

FIG. 5 illustrates an assembly for calibrating of transverse arrays in a logging tool;

FIG. 6 illustrates an assembly for calibrating longitudinal arrays in a logging tool;

FIGS. 7-8 illustrate assemblies for calibrating XY cross-component arrays; and

FIGS. 9-10 illustrate assemblies for calibrating XZ cross-component arrays.

FIGS. 11A-11B show embodiments of the disclosure in which reactances are introduced between the two housings.

DETAILED DESCRIPTION OF THE DISCLOSURE

The instrument structure provided by the present disclosure enables increased stability and accuracy in an induction wellbore logging tool and its operational capabilities, which, in turn, results in better quality and utility of wellbore data acquired during logging. The features of the present disclosure are applicable to improve the structure of a majority of known induction tools.

The disclosure will now be described in more detail and by way of example with reference to the accompanying drawings. FIG. 1 schematically shows a wellbore 1 extending into a laminated earth formation, into which wellbore an induction logging tool as used according to the present disclosure has been lowered. The wellbore in FIG. 1 extends into an earth formation which includes a hydrocarbon-bearing sand layer 3 located between an upper shale layer 5 and a higher conductivity than the hydrocarbon bearing sand layer 3. An induction logging tool 9 used in the practice of the disclosure has been lowered into the wellbore 1 via a wire line 11 extending through a blowout preventor 13 (shown schematically) located at the earth surface 15. The surface equipment 22 includes an electric power supply to provide electric power to the set of antennas 18 and a signal processor to receive and process electric signals from the receiver antennas 19. Alternatively, the power supply and/or signal processors are located in the logging tool.

The relative orientation of the wellbore 1 and the logging tool 9 with respect to the layers 3, 5, 7 is determined by two angles, one of which θ as shown in the FIG. 1. For determination of these angles see, for example, U.S. Pat. No. 5,999,883 to Gupta, et al. The logging tool 9 is provided with a set of transmitter antennas 18 and a set of receiver antennas 19, each set of antennas 18, 19 being connected to surface equipment 22 via suitable conductors (not shown) extending along the wire line 11.

The relative orientation of the wellbore 1 and the logging tool 9 with respect to the layers 3, 5, 7 is determined by two angles, one of which θ as shown in the FIG. 1. For determination of these angles see, for example, U.S. Pat. No. 5,999,883 to Gupta, et al. The logging tool 9 is provided with a set of transmitter antennas 18 and a set of receiver antennas 19, each set of antennas 18, 19 being connected to surface equipment 22 via suitable conductors (not shown) extending along the wire line 11.

Each set of antennas 18 and 19 includes three antennas (not shown), which are arranged such that the set has three magnetic dipole moments in mutually orthogonal directions, that is, in x, y and z directions. The three-antenna transmitter antenna set transmits magnetic fields T_(x), T_(y) and T_(z); the receiver antennas measure induced signal from main directions R_(x), R_(y) and R_(z) as well as the cross components, R_(xy), R_(xz) and R_(zy). Thus, antenna set 18 has magnetic dipole moments 26 a, 26 b, 26 c, and antenna set 19 has magnetic dipole moments 28 a, 28 b, 28 c. In one embodiment the transmitter antenna set 18 is electrically isolated from the receiver antenna set 19. The antennas with magnetic dipole moments 26 a and 28 a are transverse antennas, that is they are oriented so that the magnetic dipole moments are oriented perpendicular to the wellbore axis, whereby the direction of magnetic dipole moment 28 a is opposite to the direction of magnetic dipole moment 26 a. Furthermore the sets of antennas 18 and 19 are positioned substantially along the longitudinal axis of the logging tool 9.

As shown in FIG. 2A, conventional induction logging tools provide a single transmitter and receiver antenna that measure resistivity in the horizontal direction. In the mode shown in FIG. 2A, the resistivities of adjacent high resistivity sand and low resistivity shale layers appear in parallel, thus the resistivity measurement is dominated by low resistivity shale. As shown in FIGS. 1 and 2B, in the present disclosure a transverse antenna is added to measure resistivity in the vertical direction. In the vertical direction, the resistivity of the highly resistive sand and low resistivity shale are appear in series and thus the vertical series resistivity measurement is dominated by the resistivity of the highly resistive sand.

For ease of reference, normal operation of the tool 9, as shown in FIGS. 1 and 2B, will be described hereinafter only for the antennas having dipole moments in the x-direction, i.e. dipole moments 26 a and 28 a. During normal operation an alternating current of a frequency f₁ has been driven by the tool electronics (not shown) connected to the antenna 26 which, in turn, is supplied by the electric power supply of surface equipment 22 to transmitter antenna set 18 so that a magnetic field with magnetic dipole moment 26 a is induced in the formation. In an alternative embodiment, the frequency is swept through a range f₁ through f₂. This magnetic field extends into the sand layer 3 and induces a number of local eddy currents in the sand layer 3. The magnitude of the local eddy currents is dependent upon their location relative to the transmitter antenna set 18, the conductivity of the earth formation at each location, and the frequency at which the transmitter antenna set 18 is operating. In principle, the local eddy currents act as a source inducing new currents, which again induce further new currents, and so on. The currents induced into the sand layer 3 induces a response magnetic field in the formation, which is not in phase with the transmitted magnetic field, but which induces a response signal in receiver antenna set 19. The magnitude of the current induced in the sand layer 3 depends on the conductivity of the sand layer 3, the magnitude of the response current in receiver antenna set 19. The magnitude also depends on the conductivity and thereby provides an indication of the conductivity of the sand layer 3. However, the magnetic field generated by transmitter antenna set 18 not only extends into sand layer 3, but also in the wellbore fluid and in the shale layers 5 and 7 so that currents in the wellbore fluid and the shale layers 5 and 7 are induced.

The overall procedures of the present disclosure used to ensure proper functioning of a deployed multicomponent induction logging tool is summarized in FIG. 3. Calibration of the instrument's arrays is done, particularly estimating its transfer coefficient 101. Subsequently, a final verification of the tuning and calibration consistency is performed 103. This is followed by a verification of isolator sufficiency 105 for preventing an axial current flow between the tool's top and bottom housings/electronics through the feed-through pipe and conductors while logging in the boreholes filled with conductive mud.

In further detail, the fully made tool is placed in calibration area which has a small number of external parts that could interfere with magnetic and electric fields produced or received by the tool and thus affect tool readings (machinery, measurement tools, etc.). For example, positioning the tool at approximately 15 ft (4.6 m) above the ground typically reduces the tool environmental reading to a value less than about 10 mS/m. The tool is positioned parallel to the Earth with the array to be adjusted pointing normal to the ground.

FIG. 4 illustrates the BCS, comprising an assembly of conductor 401 and resistor 410, which electrically couples top housing 405 and bottom housing 404. A closed circuit is thus created from bottom housing 404 through resistor 410 through top housing 405 through a feed-through pipe running from bottom housing to top housing through mandrel 408. The value of resistor 410 can be configured to be approximately equal to a total conductivity (or resistivity) value between top and bottom housings which the tool would experience inside a borehole according to its specifications. A resistance value of approximately 20 Ohms is typically chosen.

In this arrangement the tool becomes very sensitive to the axial current that could be induced by the array transmitter in the following loop: “top housing—conductive feed-through pipe—bottom housing—BCS”. The magnitude of the current will be proportional to the array antennas displacement from their longitudinal alignment (almost true for small displacements˜1/d) and simulator resistor value.

To balance the array its transmitter antenna may be moved in the plane parallel to the ground. This antenna movement is performed until an absolute minimum in the receiver reading is reached. In one embodiment of the disclosure, the receiver antenna is positioned off-center relative to the tool. At this position, the receiver signal is particularly sensitive to misalignment of the transmitter. This makes it easier to determine the minimum. Upon adjustment the transmitter antenna frame is fixed inside the mandrel. This could be accomplished with the sets of non-conductive screws and/or with epoxy; however, alternative means could be applied, as well. Shorting the isolator between the upper housing and the mandrel is done to significantly increase the magnitude of the axial current in this test procedure and, therefore, increase accuracy of balancing. A similar positioning may be done in the vertical direction. As discussed below, the tool is more sensitive to mis-positioning in the vertical direction than in the horizontal direction. Suitable positioning screws may be provided in the logging tool to accomplish this movement.

Following the positioning of the transmitter antenna, the receiver antenna is moved to a position where the signal and the receiver antenna is zero. When this is done, the particular transmitter and receiver are properly balanced. The description above has been made with respect to movement of the antennas relative to each other. It is to be understood that when these movements are made, the antennas are also being moved relative to the feed-through pipe.

After the first horizontal array has been tuned the tool is rotated about its axis and similar procedure has been performed with next horizontal array. Generally, the instrument might have a plurality of transverse and tilted arrays so that similar tuning could be developed for each sensor. After balance of all arrays has been completed, the tool isolation short is removed and mandrel is covered with the non-conductive pressure sleeve.

Calibration of transfer coefficient is done after the instrument is positioned in the low conductive calibration environment and inserted inside the calibrator. The calibration principle lies in introducing a certain dissipative load through magnetic coupling for calibrating array so that its signal readings are identical to the values to be read while logging a homogeneous formation with finite conductivity. This is done with use of a calibrator whose electromagnetic parameters and coupling with the tool are precisely known. Using the calibrator, tool loading is achieved by the connecting certain impedance to the terminal of normally-open calibrator loop. Thus, the open loop presents an infinitely resistive formation. Conversely, by shorting, almost infinitely conductive formation is presented. Therefore, any value of the formation conductivity corresponds to its unique value of the calibration loop load.

Acquiring the calibration signal is typically done in the mode “calibration load connected—disconnected”. This difference in the tool reading indicates on how much the tool output voltage swings when the formation conductivity changes from 0 to the calibrated value. To perform calibration the tool array may be oriented normal to the ground as this leads to more consistency in measurements and apparently make its transversal arrays less sensitive to any residual noise currents that maybe circulating on the Earth surface in place of measurement (machinery, radio-stations, etc.).

After the tool transfer coefficient has been determined, the tool readings while the calibrator loop is not loaded reflect environmental conductivity and, in particular, ground conductivity. This data has to be known and stored for further processing.

The last step in calibration is verification of the tool symmetry and immunity to axial currents. The overall tool symmetry assumes that the same array reads the same values of the “ground” or environmental conductivity while its measurement direction points to ground or from the ground. For these purposes the tool is rotated around its longitudinal axis on 180°. Absence of such a “direction sensitivity” would indicate normal tool functioning and ensure respective symmetry while operating in the well bore.

For verification of the suppressing axial currents—a modified BCS test may be run with the short removed in the feed-through. Thus, connecting and disconnecting the BCS to the tool should result in absolute minimal difference in readings that would indicate for proper operation in the well without formation-dependable offset in the tool data. This modified BCS test could be run as described, or, to reduce calibration time, performed right after the transfer coefficient is determined.

Turning now to FIG. 5, one arrangement of the alignment loop is discussed. Shown therein is an alignment loop 501 surrounding an array characterized by the transmitter antenna 504 directed along an X direction (T_(x)) and the receiver antenna 508 directed along the X direction (R_(x)). Bucking antenna B_(x) 506 is also shown. This array is denoted as XX, using a nomenclature in which the first letter signifies the orientation direction of the transmitter antenna and the last letter signifies the orientation direction of the receiver antenna. This nomenclature is generally used herein. The XX and YY arrays in the multi-component tool are ideally aligned at 90° from each other. When this alignment is not met, the response of the cross components (XY, YX) are affected by part of the reading of the related main component. The alignment measuring method of the present disclosure is based on analyzing the output of the cross-component system when the tool is rotated inside of an alignment loop.

The alignment loop 501 is a stationary loop, lying so that the longitudinal axis of the loop and the longitudinal axis of the well-logging tool are substantially aligned. Its dimensions are such as to obtain substantial inductive coupling with the transmitter as well as with the receiver of both XX and YY arrays. The long “box” calibrator of FIG. 4 is used to performed calibration of the horizontal arrays. A detailed analysis of the signals is given later in this document.

FIG. 6 illustrates a loop alignment assembly usable for aligning ZZ arrays in a testing device. Transmitter TZ 601, bucking antenna BZ 603 and receiver RZ 605 are disposed along the feed-through pipe 615 and have a common longitudinal axis. Alignment loop 610 is substantially coaxial with receiver RZ 605 and substantially centered on RZ.

Cross component array calibration is discussed next. FIG. 7 illustrates an embodiment for calibration of an XY array using a calibration box. Transmitter 701 and bucking antenna 703 are disposed along the feed-through pipe oriented to produce a magnetic moment in an X-direction. Receiver 705 is disposed along the same feed-through pipe having an orientation so as to receive components of a magnetic moment in a is disposed along the same feed-through pipe having an orientation so as to receive components of a magnetic moment in Y-direction. The alignment box 710 is disposed at an angle of 45° so as to be oriented halfway between the X-direction and the Y-direction.

FIG. 8 illustrated an alternate embodiment for aligning an XY array. Alignment box 815 is located at the TX 801, and alignment box 810 is positioned at the RXY cross-component receiver 805. Both alignment boxes are oriented along the same direction as their respective transmitter/receiver. A wire 820 electrically couples alignment box 810 and alignment box 815. (in this configuration box 815 receives signal from transmitter antenna, the voltage induced across its winding produces current flowing through winding of both boxes and load impedance. While going though winding of 810 this current generates filed that is picked up by cross-component receiver)

FIG. 9 illustrates an assembly for orienting of the XZ cross-component array. Transmitter TX 901 and bucking antenna BX 903 are disposed along the feed-through pipe oriented so as to produce a magnetic moment along an X-direction. The receiver RZ 905 is disposed along the feed-through pipe and oriented so as to be receptive to Z-components of magnetic moments. The alignment box 920 can be positioned centrally between main X-transmitter 901 and Z-cross-component receiver 905 and tilted 45° with respect to the tool longitudinal axis 910. The assembly of FIG. 8 displays small signals during XZ array calibration. This signal tends to display a high sensitivity to the angle.

FIG. 10 illustrates an alternate embodiment for aligning the XZ cross-component array. Transmitter TX 1001 and bucking antenna BX 1003 are disposed along the feed-through pipe oriented so as to produce a magnetic moment along an X-direction. The receiver RZ 1005 is disposed along the feed-through pipe and oriented so as to be receptive to Z-components of magnetic moments. Alignment box 1010 is centered on transmitter TX 1001, and alignment loop 1015 is coaxial with receiver RZ 1005. A wire 1020 electrically couples alignment box 1010 and alignment loop 1015. In contrast to the assembly of FIG. 0, calibration using two alignment devices displays a large signal for the XZ array calibration.

We next discuss in detail the use of the alignment box for establishing the antenna orientation. When examining a cross-component array, the XY or YX response obtained by rotating the tool inside of the alignment loop has a zero-crossing each time that either a transmitter or a receiver antenna is perpendicular to the plane of the loop. Whichever antenna (transmitter or receiver) is substantially aligned with the loop (enclosed in the same plane) experiences a maximum coupling with the alignment loop. When the position of the aligned antenna is varied around the point of alignment with the alignment loop, the coupling response between them undergoes a slow change corresponding to the variation. The non-aligned antenna experiences a minimum coupling with the alignment loop. When the position of the non-aligned antenna is varied around this point of minimal coupling, the coupling experiences an abrupt change. The coupling becomes zero when the non-aligned antenna achieves perpendicularity with the alignment loop. A practitioner in the art would recognize that the zero-crossings of the coupling response are significantly affected by the antenna that is at right angle to the alignment loop, regardless of whether the perpendicular antenna is a receiver or a transmitter. The substantially aligned antenna plays little or no role in the production of a zero-crossing. The angle between successive zero crossings thereby represents an alignment angle between the two related antennas.

Mathematically, the inductive coupling between two antennas resembles a cosine function of the angle between them. Thus, the coupling response system of antennas made by an aligned system of cross components and an alignment loop is given by the following expression:

$\begin{matrix} {{R(\phi)} = {K \cdot {\cos(\phi)} \cdot {{\cos\left( {\phi - \frac{\pi}{2}} \right)}.}}} & {(1).} \end{matrix}$ Applying trigonometric identities, Eq. (1) can be simplified to R(φ)=K·cos(φ)·sin(φ),  (2). and since

$\begin{matrix} {{{{\sin(\phi)} \cdot {\cos(\phi)}} = {\frac{1}{2}{\sin\left( {2 \cdot \phi} \right)}}},} & {(3),} \end{matrix}$ it follows that

$\begin{matrix} {{R(\phi)} = {K \cdot \frac{1}{2} \cdot {{\sin\left( {2 \cdot \phi} \right)}.}}} & {(4).} \end{matrix}$ Eqn. (4) illustrates that there are two cycles of variation for each cycle of tool rotation.

By considering a misalignment angle β between transmitter and receiver, the response function can now be expressed as

$\begin{matrix} {{{R\left( {\phi,\beta} \right)} = {K \cdot {\cos(\phi)} \cdot {\cos\left( {\phi - \frac{\pi}{2} + \beta} \right)}}},} & {(5),} \end{matrix}$ where each cosine function characterizes the response of the individual cross component antennas. It is easy to see that

$\begin{matrix} {{{R\left( {\phi,\beta} \right)} = 0},{when}} & (6) \\ {{\phi = {n \cdot \frac{\pi}{2}}}{{or}\mspace{14mu}{when}}{{{\phi - \frac{\pi}{2} + \beta} = {{{n \cdot \frac{\pi}{2}}\mspace{14mu}{with}\mspace{14mu} n} = {\pm 1}}},2,3,\ldots}} & {{Eq}.\mspace{14mu}(7)} \end{matrix}$ According to eqn. (7), the angle between successive zero-crossings represents the alignment angle among the cross component antennas. An intuitive graphical approach can therefore be used to measure the misalignment angle between transmitter and receiver.

Alternatively, the misalignment angle can be obtained simply by using a trigonometric regression function to analyze the response of the system. Applying trigonometric identities to Eqn. (5), the response of the misaligned system can be written as

$\begin{matrix} {{{R\left( {\phi,\beta} \right)} = {{K \cdot {\cos(\phi)} \cdot {\sin(\phi)} \cdot {\cos(\beta)}} + {K \cdot {\cos^{2}(\phi)} \cdot {\sin(\beta)}}}}{{R\left( {\phi,\beta} \right)} = {{K \cdot \frac{1}{2} \cdot {\sin\left( {2 \cdot \phi} \right)} \cdot {\cos(\beta)}} + {K \cdot {\cos^{2}(\phi)} \cdot {\sin(\beta)}}}}{{R\left( {\phi,\beta} \right)} = {{\frac{K}{2} \cdot {\sin\left( {{2 \cdot \phi} + \beta} \right)}} + {\frac{K}{2} \cdot {\sin(\beta)}}}}} & (8) \end{matrix}$ The last expression in eqn. (8) indicates that a graphical representation of the coupling response of the misaligned cross component system resembles a sinusoidal function. The period of this sinusoid equals 180° and has offsets on both the abscissa and the ordinate. The offset on the abscissa is β, and the offset on the ordinate is (K/2)sin(β). Also, the coupling response is of the form A sin(x+B)+C, where A=K/2, B=β and C=(K/2)(sin(β). The coefficient B obtained with such fitting represents the misalignment angle. The cross component response can thus be fit to this curve.

The sensitivity to possible displacement along the tool's longitudinal axis or vertically can be analyzed by changes in the product M=M_(T-C)M_(C-R), where M_(T-C) is the mutual inductance between the transmitter and the alignment antennas, and M_(R-C) is the mutual inductance between the alignment and the receiver antennas. Table 1 illustrates mutual inductances that result from misalignment or displacement of an alignment antenna in the horizontal direction (longitudinally). There is in general a flexibility of 1″ without substantially affecting the induction response.

TABLE 1 Calibrator Displacement M_(T-C) M_(C-R) M [inch] [microHenry] [microHenry] [μH]² 4 13.348 16.700 222.912 2 13.409 13.580 182.094 1 13.443 13.521 181.763 ¾ 13.452 13.510 181.736 ½ 13.461 13.499 181.710 0 13.479 13.479 181.683 −½ 13.499 13.461 181.710 −¾ 13.510 13.452 181.736 −1   13.521 13.443 181.763 −2   13.580 13.409 182.094 −4   16.700 13.348 222.912

Table 2 shows the effects of misalignment in the vertical direction. A misalignment exceeding 5/16″ produces an error greater than 0.22%. Thus vertical misalignment has a greater effect on induction response than horizontal misalignment.

TABLE 2 Calibrator Displacement M_(T-C) M_(C-R) M [inch] [microHenry] [microHenry] [μH]² % 0 13.479 13.479 181.683 0 3/16 13.474 13.474 181.549 0.074 5/16 13.464 13.464 181.279 0.22 7/16 13.449 13.449 180.876 0.44

To properly position the arrays, the transmitter antenna of one array is moved in the direction normal to the ground. This antenna movement is performed until an absolute minimum in the coupling response is determined. Upon adjustment, the transmitter antenna frame is fixed inside the mandrel. After the first horizontal array has been tuned, the tool is rotated on its axis and a similar procedure is performed with the other horizontal array. Generally, similar tuning can be developed for an instrument having a plurality of transverse and tilted arrays. After balance of all arrays has been achieved, the tool isolation short is removed and mandrel is covered with the non-conductive pressure sleeve to protect induction antennas from being directly exposed to borehole fluids.

A final verification of the antenna balancing and calibration consistency is made. Calibration of a transfer coefficient is performed once the instrument is inserted inside the calibrator in the low conductive calibration environment. A magnetic load is introduced suitable for calibrating array, so that its signal readings are identical to the values to be read while logging a homogeneous formation. The magnetic load is introduced using the above-referenced calibrator using known electromagnetic parameters and coupling parameters. The tool loading can be achieved by connecting selected impedance to the terminal of a normally-open calibrator loop. Thus, the open loop represents an infinitely resistive formation. Once shorted, the closed loop represents an almost infinitely conductive formation (limited only by internal impedance of the wires of the calibrator loop). Therefore, a calibration loop load can be chosen effectively representing a given formation conductivity values.

Those versed in the art and having benefit of the present disclosure would recognize that the coupling of the first conductive housing to the second conductive housing effectively produces an antenna which produces a magnetic field at the first receiver that is substantially equal to the magnetic field that would be produced by axially flowing currents with the logging tool in the borehole. In one embodiment of the disclosure, the axially flowing currents are reduced so that at the operating frequency of the induction logging tool. This can be done in one of two ways.

In the first way, an inductance 1105 is introduced in the flow path 1101 for the axially flowing currents. This acts as a high cut filter, with a cutoff frequency related to the reactance of the impedance, so that if the operating frequency of the transmitter is above the cut-off frequency, the magnetic field produced by the axially flowing currents at the receiver antenna is reduced.

In the second way, a capacitance 1103 is introduced in the flow path 1101 for axially flowing currents. This acts as low-cut filter with a cutoff frequency related to the reactance of the capacitance, so that if the operating frequency of the transmitter is below the cut-off frequency, the magnetic field produced by the axially flowing currents at the receiver antenna is reduced. A simple way to introduce such a capacitance is to introduce a gap filled with a non-conducting material in the mandrel, the through cables and all other paths for axial currents.

Implicit in the control and processing of the data is the use of a computer program on a suitable machine readable medium that enables the processor to perform the control and processing. The machine readable medium may include ROMs, EPROMs, EEPROMs, Flash Memories and Optical disks.

While the foregoing disclosure is directed to the specific embodiments of the disclosure, various modifications will be apparent to those skilled in the art. It is intended that all variations within the scope and spirit of the appended claims be embraced by the foregoing disclosure. 

1. A method of using an induction logging tool having an axial flow path for currents, the method comprising: (a) introducing a reactance in the axial flow path; and (b) operating a transmitter at a frequency related to a cutoff frequency defined by the introduced reactance.
 2. The method of claim 1 wherein introducing the reactance further comprises introducing an inductor, the method further comprising operating the transmitter at a frequency above the cutoff frequency.
 3. The method of claim 1 wherein introducing the reactance further comprises introducing capacitor, the method further comprising operating the transmitter at a frequency below the cutoff frequency.
 4. The method of claim 1 further comprising using, for the logging tool, a multicomponent tool having a plurality of transmitter antennas and a plurality of receiver antennas, and wherein a first antenna of the plurality of transmitter antennas has an axis that is one of (i) substantially parallel to a longitudinal axis of the tool, or (ii) substantially orthogonal to a longitudinal axis of the tool.
 5. The method of claim 1 further comprising using, for the logging tool, a multicomponent tool having a plurality of transmitter antennas and a plurality of receiver antennas, and wherein a first antenna of the plurality of receiver antenna has an axis that is one of (i) substantially parallel to a longitudinal axis of the tool, or (ii) substantially orthogonal to a longitudinal axis of the tool.
 6. An apparatus for evaluating an earth formation, the apparatus comprising: (a) an induction logging tool configured to be conveyed in a borehole; (b) at least one transmitter antenna on a first housing configured to produce an electromagnetic wave in the earth formation; (c) at least one receiver antenna on a second housing configured to produce a signal responsive to the electromagnetic wave; (d) a current flow path between the first housing and the second housing, the current flow path having a reactance; and (e) a processor configured to: (I) operate the at least one transmitter antenna at a frequency related to the reactance; and (II) estimate from the produced signal a resistivity property of the formation.
 7. The apparatus of claim 6 wherein the reactance comprises an inductor and wherein the processor is further configured to operate the at least one transmitter antenna at a frequency above a cutoff frequency defined by the inductor.
 8. The apparatus of claim 6 wherein the reactance comprises a capacitor and wherein the processor is further configured to operate the at least one transmitter antenna at a frequency below a cutoff frequency defined by the capacitor.
 9. The apparatus of claim 6 wherein the at least one transmitter antenna comprises a plurality of transmitter antennas.
 10. The apparatus of claim 6 wherein the at least one receiver antenna comprises a plurality of receiver antennas. 